Decade Resources Ltd V.DEC

eskay creek potential was seen as far back as 2006

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Mineral occurrences on the Del Norte property, with the exception of the Crackle and Horatio Zones, are mainly vein type areas of quartz flooding, brecciation and sulphidation focused along a contact between older Hazelton Group volcanic rocks and younger basinal sediments of the Salmon River Formation or Bowser Lake Group. The contact is mainly tectonic but the fault structures are coincident with the stratigraphic contact between these units, possibly due to structural weakness caused by early faulting during the basin initiation. The occurrence of a patchy but intense acid-leach alteration system, stratigraphically beneath the sediment/volcanic contact, may be a source of metals which were then precipitated in the more permeable tectonically disrupted rocks at the contact. The Bullion area, "3 oz" Vein and SP Veins are promising fault associated prospects.

Establishing a continuum at Del Norte between silver and gold-rich vein type mineralization and precious metal-enriched exhalativc mineralization typifying the Eskay Creek Deposit remains a priority for the 2006 exploration program.

Harvey Klatt, P.Gco. is the Qualified Person for Sabina in charge of the 2006 exploration program on the Del Nortc property

https://propertyfile.gov.bc.ca/reports/PF882313.pdf